Quartz, Quartz epimorph after Fluorite

This specimen features an aesthetic grouping of sharp quartz epimorphs that have formed after what is believed to have been fluorite, displaying softly-defined dodecahedral forms. The quartz formations are hollow, as evident from the incomplete crystals, which offer a fascinating glimpse into the mineral’s unique growth process.

The specimen was collected during a trip to a locality known as Gringo Gulch, near Patagonia, Arizona. This area is known for its distinctive mineral occurrences, particularly for amethyst crystals and now for these intriguing quartz epimorphs. For a detailed account of the collecting trip and more information on this locality, you can read the full story of our discovery here: Collecting Quartz Epimorphs Near Patagonia, AZ.